Open Access Article
Stefan Andrei
Irimiciuc
*ab,
Sergei
Chertopalov
a,
Veronica
Goian
a,
Esther
de Prado
a,
Martin
Vondráček
a,
Eva
Marešová
a,
Petr
Svora
a,
Ladislav
Fekete
a,
Mariana
Klementová
a,
Stanislav
Kamba
a and
Ján
Lančok
a
aInstitute of Physics of the Czech Academy of Sciences, Na Slovance 1999/2, Prague, Czech Republic. E-mail: irimiciuc@fzu.cz
bNational Institute for Laser, Plasma and Radiation Physics – NILPRP, 409 Atomistilor Street, Bucharest, Romania
First published on 14th October 2025
The role of ambient gas in the epitaxial growth of manganese oxides on MgO by pulsed laser deposition was investigated by performing complex morphological and structural characterization of thin films while simultaneously monitoring the growth process with electrical probes. The growth in N2 atmospheres leads to the formation of highly oriented MnO coatings that present compressive in-line stress and contain highly oriented defects, which are induced during growth by the high kinetic energy of the plasma. The presence of O2 during unlocks the growth of highly crystalline Mn3O4 rotated by 45 deg to MgO, with X-ray photoelectron spectroscopy (XPS) measurements showing the contribution of the MnO bonding states on the surface on Mn3O4 due to ambient contamination of the sample. The ability of each atmosphere to promote the growth of two selected oxide phases was shown by both ellipsometry and infrared spectroscopy measurements. The in situ monitoring of growth highlights the ion acceleration caused by the use of N2 compared with O2 and the formation of a plasma environment that is optimal for the formation of molecular species as well as a strong oxide contribution to growth.
A special class of coatings that were reportedly manufactured with great success via PLD are based on manganese oxides.27–29 A wide range of reported manganese oxide films have been proposed for applications ranging from lithium-ion batteries30 to aqueous flow batteries,31 oxygen evolution electrocatalysts29 or thermochemical water splitting.32 The key characteristics that make manganese oxides essential for these applications are their oxidation states and diverse polymorphisms, which also pose an important challenge in predicting the phase that will form under specific processing conditions. Studies on PLD growth of manganese oxides have explored limited regions of the phase space. Films from a MnO target formed Mn2O3 at 550–700 °C and Mn3O4 at 700–850 °C under 1–10 Pa O2, differing quantitatively from bulk phase diagrams.33 Reports on routes or MnxOy phase formation from a Mn target at substrate temperature of 600 °C yielded Mn2O3 at 1 Pa, Mn3O4 at 10 Pa, and MnO in vacuum (10−3 Pa).34 Deposition from MnO2 at 10 Pa produced MnO2 phases at 300–450 °C and Mn2O3 at 550–650 °C. Mn and Mn3O4 targets ablated at 200–700 °C and 10−5–50 Pa formed Mn2O3 and/or Mn3O4. Sputtering studies similarly showed that temperature, oxygen pressure, and morphology critically control oxidation state and performance.28 Additionally, to reach epitaxial growth of various MnxOy phases, other techniques have shown great promise such as atomic layer deposition (ALD)35,36 with a wide range of strategies to obtain epitaxial growth such as target phase tailoring33,37 or introduction of intermediary Pd layers.38
Our work focused on investigating the role of N2 and O2 atmospheres in the deposition of MnO thin films by pulsed laser deposition. Structural and morphological characterization of the films revealed preferential growth of the epitaxial MnO phase in N2 and Mn3O4 in an O2 atmosphere. The deposition was monitored by an angle- and time-resolved Langmuir probe. The background gas nature affects the kinetic energies of the ions as well as the structure of the time-of-arrival currents. Features of oxidation are observed throughout the measurements, with clear enhancement in plasma kinetics in the case of N2, which acts as an accelerating medium for the MnO plasma.
MnxOy thin films were deposited on MgO (100) substrates positioned 50 mm from the target via 6000 consecutive pulses at 650 °C under identical irradiation conditions at selected O2 and N2 pressures. The transmittance spectra of the resulting films were measured by a spectrometer (USB4000, Ocean Optics) in the spectral range from 300 to 890 nm. The light source (DT-mini-2-GS, Ocean Optics) was coupled with a focusing lens by an optical fiber with a 200 μm core diameter. The light spot diameter on the sample was approximately 2 mm, which determined the lateral resolution of the transmittance measurement. AFM (AFM Dimension ICON, Bruker) was used to investigate the surface morphology, roughness and thin film thickness. The measurements were performed under ambient conditions, and images were obtained in peak force tapping mode using ScanAsystAir tips with a scan area of 1 × 1 μm2.
X-Ray diffraction (XRD) measurements were performed using three different diffractometers. The samples were examined with an X-ray diffractometer (Empyrean, Malvern Panalytical) with monochromated Cu Kα radiation (wavelength λ = 1.54151 Å, U = 45 kV, I = 30 mA) in grazing incidence XRD mode. The incident angle was 0.85°, which corresponds to ∼10 mm of sample irradiation. The XRD measurements were made at the central part of the deposited film with an area of 10 × 10 mm2. High-resolution XRD (HRXRD) measurements were carried out via a SmartLab SE Multipurpose diffractometer (Rigaku Corp., Tokyo, Japan) with Cu Kα1 radiation. The incident beam optics included a parabolic Göbel mirror and a two-bounce Ge (220) monochromator. For the diffracted beam, a 2.5° Soller slit and a HyPix-3000 2D detector operating in 0D mode were utilized. Finally, pole figures were obtained via an X’Pert Pro PANalytical diffractometer (PANalytical B.V., Almelo, Netherlands) with Co Kα radiation, which was configured with a point-focus X-ray source and an X’Celerator detector.
The composition of the films was investigated via an XPS NanoESCA Omicron Nanotechnology instrument. Monochromatic Al anode Kα radiation (E = 1486.7 eV) was used as an X-ray source. The analyzed spot size was 100 × 300 μm2, and several positions on the sample were probed. For depth profiling, Ar+ sputtering was performed at 2 × 10−4 Pa, an accelerating voltage of 3 keV and an ion incidence angle of 15° with respect to the sample surface normal. One-minute depth profiling removed approximately 0.5/1 nm of the thickness of the material. Spectral fitting was conducted via CasaXPS software. Measurements were performed in a mode with 0.5 eV energy resolution.
Transmission electron microscopy (TEM) was carried out on an FEI Tecnai TF20 X-twin microscope operated at 200 kV (FEG, 2.5 Å point resolution) equipped with an EDAX energy dispersive X-ray (EDX) detector (30 mm2, 135 eV resolution) and a Gatan imaging filter (GIF) Quantum for electron energy loss spectroscopy (EELS). The microscope was also used in scanning mode (STEM) with a high-angle annular dark field detector (HAADF). TEM images, selected-area electron diffraction (SAED) patterns, and EELS spectra were recorded on a Gatan UltraScan CCD camera via the Digital Micrograph software package. SAED patterns were evaluated via CrysTBox software. The EELS data were collected in STEM mode with a 5 mrad convergence angle, a 10 mrad collection angle, and an energy resolution of 1.2 eV. EELS quantification was performed via the Digital Micrograph software package. Lamellas for the TEM observations were prepared via the focused-ion beam technique using an FEI Quanta 3D with a Ga source.
IR reflectivity spectra were obtained at room temperature using a Fourier transform IR spectrometer Bruker IFS 113v in the frequency range of 30–3000 cm−1. Reflectance measurements were performed in near-normal incidence geometry. In the far and middle IR frequency ranges, two deuterated triglycine sulfate detectors were used.
For the films deposited in N2 atmospheres, the transparency regime is indicated by film thickness interferences with average transmittance (350–900 nm) of 70–80%, whereas coatings deposited in high-pressure O2 have a reduced transmission of approximately 10% (Fig. 2(a)). By implementing the Tauc plot method, the direct band gaps were estimated. For the N2 case, the band gap increases in the 3.9–4.33 eV range with increasing N2 pressure from 10−2 to 10 Pa, whereas for the O2 case, it increases from 1.1–1.9 eV in the same pressure range. It is clear that a N2 atmosphere generates a MnO phase, whereas O2 generates a Mn3O4 phase with specific defects. According to,41,42 band gap values above 4 eV are induced by O vacancies, which implies the following reaction:
. This is understandable for our deposition conditions, as the N2 atmosphere limits O2 inclusion in the MnO films. For the films deposited in an O2 atmosphere, the band gap value implies the presence of Mn vacancies with two associated electrons.
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| Fig. 2 Transmittance spectra of MnO films (a) and ellipsometry data (b) (refractive index and extinction coefficient). | ||
Ellipsometry measurements were used to determine the optical constants (n and k) and optical band gap (Eg) of thin layers of MnO and Mn3O4. The optical model used to characterize the samples consists of a MgO substrate, a MnO/Mn3O4 thin layer and surface roughness. This model best defines the structure of the samples, as it provides the best fit. It can be seen from Fig. 2(b) that the thin films of MnO and Mn3O4 are transparent over some part of the measured spectral range (MnO λ > 650 nm, Mn3O4λ > 350 nm). This was used as a starting point for initial analysis of the approximate values of the refractive index and thickness (Cauchy model). For comparison, the thickness of the layers was measured on a KLA Tencor profilometer (between 180 nm and 200 nm depending on the growth conditions, more details are given in Fig. S2 and S3). The measured values were consistent with the optical data. To describe optical dispersion over a wide wavelength range, the model was improved by including 1 Tauc–Lorentz oscillator and 1 Gaussian oscillator. The optical band gap (Eg) was determined from the Tauc–Lorentz formula, which was found to be Eg(MnO) = 4.0 and Eg(Mn3O4) = 1.9. The optical constants n and k of the MnO and Mn3O4 thin layers derived from SE analysis are presented in Fig. 2(b).
Accurate MnO phase identification can be rather difficult because of the large number of available oxidation states.43 Kerisit et al. provide a comprehensive empirical path to phase differentiation. The shape of the Mn 2p peak is similar to that reported by,28,36 who investigated the influence of the nature of MnO (island, film, bulk) on the shape and structure of the Mn 2p peak. By following the fitting procedure for Mn 2p,43 a 5 peak deconvolution was used (Fig. 3(b)), which first tentatively confirms the presence of the MnO phase. The possible oxidation states available can be identified from the presence of high-BE satellites in the 2p region, such as those indicated in Fig. 3(a). These satellites are unique identifying features of the Mn 2p peak and are positioned at a 6.15 eV higher binding energy. These findings are in good agreement with the Mn 2p core level spectra reported in the literature for MnO(001) films.33 Moreover, the multiplet splitting energy (Δ) of the Mn 3s peak can be used as a quantitative indicator of the Mn oxidation state: MnO (6.1 eV), Mn3O4 (5.7 eV), Mn2O3 (5.4 eV), and MnO2 (4.4 eV); however, overlap of the Mn 3s and Mg 2s peaks necessitates deconvolution for MnOx thin films on MgO. The observed multiplet splitting (Fig. S4b) for the N2 case is approximately 5.7 eV, whereas for the O2 case, 6.1 eV is consistent with bulk MnO, and the area ratio of the parallel (low-energy) and antiparallel (high-energy) Mn 3s peaks is ∼1.6, which is slightly above the predicted value of 1.4. This result implies the preferential formation of the MnO phase in the samples grown in a N2 atmosphere, whereas the samples grown in O2 have a smaller energy split characteristic of the formation of Mn3O4. Moreover, there is a 2
:
1 peak area ratio in the 3s XPS spectra of paramagnetic 3d transition metals arises from many-body effects beyond simple exchange interaction, which create two final states from the interaction between the core hole and the unpaired valence electrons. The observed 2
:
1 intensity distribution reflects the statistical degeneracy of these multi-electron states, with the lower energy peak often having a higher intensity due to these complex atomic and electronic correlation effects. This conclusion is confirmed by the data presented in Fig. S4(a) and (b), where it can be seen that MnO satellites are present only in the as-received samples deposited in a N2 atmosphere. The results are in good agreement with the optical transmission and ellipsometry investigations previously discussed.
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| Fig. 3 XPS spectra of Mn2p for various deposition conditions (a) and the 5 peak fit characteristics for MnO (b). | ||
The samples deposited at 0.1 Pa O2 and 0.1 Pa N2 were selected for further analysis because of their similar dynamic deposition regimes. Fig. 4(a) shows the symmetric ω–2θ scans on a quadratic scale for the selected samples, with the vertical axis truncated for better visualization due to the extremely high intensity of the substrate. Both films are oriented out-of-plane in the same direction as the substrate and exhibit a unique phase, cubic MnO for deposition in a N2 atmosphere or tetragonal Mn3O4 in the case of O2. Two key observations can be highlighted: the diffraction peaks of MnO are asymmetric on the right side, a phenomenon related to defects, as indicated by transmission measurements. On the other hand, a greater width of the diffraction peaks can be observed in the case of Mn3O4, indicating a higher microstrain, along with a notably lower intensity. The crystalline quality of the layer, understood as the out-of-plane misorientation, was explored through rocking curve (ω scan) measurements of the symmetric 002 reflection. The results are shown in Fig. 4(b). MnO exhibited a full width at half maximum (FWHM) of approximately 0.5°, indicating good crystalline quality; in contrast, Mn3O4 showed a significantly larger FWHM, reflecting lower quality.
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| Fig. 4 HRXRD measurements as a function of the growth atmosphere: (a) ω–2θ scans and (b) rocking curves. The peaks are indexed according to their phase and (hkl). The vertical axis in Fig. 4(a) is truncated for better visualization. | ||
The texture of the samples was examined through pole figure measurements, with the results on a logarithmic scale shown in Fig. 5. Pole figures for the (002), (022), and (111) reflections of MnO are presented in Fig. 5(a)–(c), respectively. No additional spots beyond those expected for a cubic structure are observed: one pole for the symmetric (002) reflection and four poles spaced azimuthally 90° apart at χ ≈ 45° for the (022) reflection and at χ ≈ 54.74° for the (111) reflection. Similarly, no additional features are observed in the pole figures for the Mn3O4 layer, corresponding to the (004), (033), and (224) reflections, as shown in Fig. 5(c)–(e), respectively. The additional spots visible in these figures are due to the tails of various diffraction peaks from MgO.
From the results shown above, we can conclude that the films grow epitaxially and without twins. In the case of MnO, the growth occurs as cubes on cubes, whereas the Mn3O4 layer grows with its lattice 45° azimuthally rotated relative to the substrate. Therefore, the epitaxial relationships are as follows:
| (001)MnO||(001)MgO, [100]MnO||[100]MgO |
| (001)Mn3O4||(001)MgO, [100]Mn3O4||[110]MgO |
The in-plane a- and out-of-plane c-lattice parameters were determined from reciprocal space maps (RSMs). Fig. 6(a) and (b) display the (002) symmetric and (024) asymmetric RSMs for the MnO layer, respectively. Upon visual inspection of the asymmetric RSM, it is evident that the layer is very relaxed. The (002) symmetric RSM for the Mn3O4 layer is shown in Fig. 6(c), and the asymmetric (228) RSM is shown in Fig. 6(d). Owing to the rotation of the lattice, the relaxation state of the Mn3O4 layer cannot be inferred from the asymmetric RSM, as the corresponding (228) reciprocal space point of the substrate appears at a different azimuth. In the inset of this figure, a wide snapshot of the reciprocal space is shown, where the (204) reflection of the substrate is visible, confirming the accuracy of the measurement.
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| Fig. 6 Symmetric (a) and (c) and asymmetric (b) and (d) reciprocal space maps of the films: MnO (a) and (b) and Mn3O4 (c) and (d). | ||
In the case of MnO, the lattice mismatch imposed by the substrate (approximately 5%) induces a biaxial stress that modifies the structure of the film. As a consequence, a compressive in-plane strain is present. The calculated in-plane a- and out-of-plane c-lattice parameters, along with the corresponding tabulated values and the resulting strains, are summarized in Table 1.
| Sample ID | Phase | a (Å) | c (Å) | e (%) in-plane | e (%) out-of-plane |
|---|---|---|---|---|---|
| 0.1 Pa N2 | MnO | 4.433 | 4.455 | −0.29 | 0.20 |
| PDF 04-005-4310 | MnO | 4.446 | |||
| 0.1 Pa O2 | Mn3O4 | 5.704 | 9.585 | −0.30 | −0.25 |
| PDF-04-007-1841 | Mn3O4 | 5.765 | 9.442 |
Lamellas from two samples (0.1 Pa N2 and 0.1 Pa O2) were studied in detail via TEM methods: imaging (including HRTEM), electron diffraction (Fig. 7) and spectroscopy (Fig. 8).
The overall appearance of the two samples is quite different (Fig. S5). The N2 sample shows strong contrast variations that might signify strain or other changes in the structure, such as the presence of defects. In addition, the surface of a sample is not perfectly flat and displays dips and dents. In contrast, the O2 sample has a flat surface and appears more homogeneous. The thickness of the layers differ between the two samples. The peak width was 188 nm for the N2 sample and 245 nm for the O2 sample.
From the SAED patterns (Fig. 7), the structures of both the layer and the substrate were investigated, as were their mutual growth relationships. In the layer of the N2 sample, all high-intensity diffraction spots correspond well to cubic MnO. However, there are additional low-intensity diffraction spots present in the positions of reflections (110), (310), etc., which violate the extinction rules for F-centering in cubic MnO. To explain the presence of these spots, we also tested matching the experimental SAED patterns against simulated tetragonal Mn3O4 diffraction patterns (Fig. S6). We were able to reproduce the additional spots; nevertheless, to match, the unit-cell parameters had to be reduced by 9%, which is too much even for electron diffraction.
Bright-field and dark-field (made with 110 diffraction spots) images highlight inhomogeneities in the layer (Fig. 8). Cone structures with the base connected to the interface with the MgO substrate and narrowing as layer growth progresses are displayed. These structures are composed of defects perpendicular to the (110) direction in MnO, which cause partial loss of periodicity and appear as extinction-violation diffraction spots in the SAED patterns. They reflect the misfit of the MgO substrate and the MnO layer at the initial state of growth, which later relaxes as the layer grows into the more periodic structure. This is documented by the FFTs of the HRTEM image (Fig. S7), where the FFT spots from MgO and well-ordered MnO (area 1) are sharp, whereas the FFT spots from area 2 containing many defects diffuse, reflecting the partial loss of periodicity.
The chemical composition of the layers was studied via EDX and EELS. The main reason was the uncertainty in the phase composition of the layer in the N2 sample. Mn-oxides exist in several forms: MnO (50/50 ratio), Mn3O4 (43/57 ratio) and Mn2O3 (40/60 ratio). The EDX profiles (Fig. S8) show a homogeneous distribution across the layer but yield unrealistic compositions for Mn-oxides, e.g., Mn/O ratios of 30/70 for Mn3O4 and 40/60 for MnO, whereas the composition of MgO corresponds to the perfect 50/50 ratio. This is caused by strong MnL/OK peak overlap in the EDX data (OK – 0.525 keV, MnL – 0.556 keV, 0.637 keV). Therefore, EELS was employed to obtain the correct results (Fig. S9). In EELS, the edges are well separated (OK – 532 eV, MnL1 – 651 eV, MnL – 640 eV). Indeed, the EEL spectra give composition ratios close to the expected values of 49(3)/51(3) for MnO and 43(2)/57(3) for Mn3O4 (Fig. 8). In addition, we searched for some variations between the perfect MnO and defective MnO in the N2 sample, but no such variation was detected, as shown in the profile in Fig. S7.
The layer of the O2 sample is formed by tetragonal Mn3O4 with the growth relationship rotated by 45 deg to the MgO substrate: MgO[001]||Mn3O4[110], MgO(200)||Mn3O4(−220) (Fig. 8). The layer is homogeneous, and the chemical composition according to the EEL spectrum corresponds to Mn3O4 (Fig. 8).
The IR reflectance spectra of thin films prepared in various O2 and N2 atmospheres with different partial pressures were measured, and the results are presented in Fig. 9. Notably, the IR reflectance spectra can offer fast and accurate information about the chemical composition of the thin layer because different Mn oxides have completely different selection rules for the activity of polar phonons. IR spectra are sensitive to phonons even in films with thicknesses less than 50 nm.44 The spectra of only the films produced at 0.1 Pa of O2 and N2 and the bare (100) MgO substrate exhibit a broad reflection band (restrahlband) between 400 and 750 cm−1 (see the black curve). Since MgO crystallizes in a simple rock salt structure, it has only one IR-active phonon allowed by symmetry, which we see at ∼400 cm−1
45 (the transverse optical frequency of this mode). The decrease in reflectivity at ∼750 cm−1 corresponds to the longitudinal phonon frequency of the same optical mode, and the weak minimum at 650 cm−1 appears due to multiphonon absorption. The increase in reflectivity below 100 cm−1 is due to reflection from the back of the 1 mm thick MgO wafer, as the substrate becomes IR transparent in this region. The IR spectrum of the thin film grown in a N2 atmosphere (red curve) shows one additional reflective band near 274 cm−1, in addition to the reflective band from MgO. This indicates that the film is MnO, since this material, like MgO, has only one IR-active optical phonon. Its frequency corresponds well to that observed in the MnO crystal.46 Previously published IR spectra of MnO thin films on MgO show slightly different phonon frequencies because the films in45 experienced a strain that shifted the phonon frequency in MnO.
The spectra of the films grown in an O2 atmosphere are more complex, with three peaks below 250 cm−1 and two minima at 470 and 600 cm−1, in addition to the MgO response. Their frequencies correspond to the phonon frequencies of the thin film. In fact, if the TO phonon frequencies of the film lie below the TO frequency of the substrate, they appear as reflection peaks in the IR spectrum. However, if the phonon frequencies of the film lie within the restrahlband of the substrate, they appear as minima in the reflection spectra.44 From the number of phonons in the thin film, it is clear that this layer cannot be MnO. However, the phonon frequencies correspond well to the stronger phonons in Mn3O4.47
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| Fig. 10 Selected current charge temporal traces for MnO plasma expansion in O2 (a) and N2 (b) atmospheres and their respective charge density velocity distributions (c), (d). | ||
In Fig. 10(b) and (c), the charge density velocity distributions are shown, according to the procedure from.51,52 The expansion velocity of the plasma increases as the O2 and N2 pressures increase to 2 Pa, followed by a decrease in the high pressure region. This is due to the ionization of the working gas, which leads to the formation of an accelerating double layer in front of the plasma. The acceleration of the ions has a threshold at 2 Pa, which results in a reduction in the expansion velocity, with 11% in the N2 case and 24% in the O2 case. Overall, the expansion velocities derived for MnO expansion in N2 are higher than those in O2 by a factor of 2. This is due to the local acceleration of selected species in front of the plasma. The ionization of the N2 atmosphere leads to the presence of N+, which predominantly accelerates negative charges in the plasma. The deceleration of the plasma above 2 Pa coincides with a mean free path from 3.5 mm, which defines highly collisional regime movement in the PLD geometry of the reaction chamber. The ionization of working gas and understanding the subsequent role of N2 in deposition are key aspects in explaining the phase tailoring during growth. During deposition, a N ionized cloud is generated at the front of the expanding MnO plasma; thus, the deposited film will be passivated by N2. The subsequent pulses, owing to their higher energy, will therefore clean the adsorbed N2 molecules from the surface, allowing the deposition of the pure MnO phase.
Using the approach from24,50,51 in Fig. 11, we plotted pressure-angle maps of the kinetic energy of the two main ionic groups and Mn− densities in the laser-produced plasmas. The highly kinetic ionic group is defined by energies in the 500–650 eV range in low-pressure oxygen environments of 10−4–2 Pa, followed by a decrease to 70 eV in all expansion directions. The low kinetic group is defined by a multipeak structure with a first peak at 0.1 Pa O2 and a second peak at 2 Pa and 10 Pa. The maximum values are reached above 2 Pa and are in the 30–40 eV range. On the larger expansion axis, a two-maxima distribution is observed, with the first peak at 12 eV observed at 10−4 Pa and the second peak at 0.1 Pa at 15 eV. A major aspect that needs underlining is the fact that the high and low kinetic groups have a complementary distribution. The low-energy kinetic group is dominant at high O2 pressures, whereas the high-energy kinetic group is dominant at low pressures. With O2 addition above 2 Pa, strong thermalization of the plasma occurs. The thermalization process53 involves increasing the collision rate of the ions and thus secondary ionization processes. The kinetic energy of both ionic groups is greater than the individual ionization energies of the Mn (7.34 eV) and O (13.6 eV) atoms as well as the dissociation energies of the O2 and MnO bonds. This conclusion is supported by the quasi exponential increase in the ion density, with a maximum of 6.5 × 1013 cm−3 at 5 Pa.
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| Fig. 11 Pressure and angle mapping of kinetic energy and ion density for plasma generated under various O2 (a)–(c) and N2 (d)–(f) conditions. | ||
In the N2 case, the high kinetic energy group has a maximum (5.5 keV) at 0–5° at 10−4–10−2 Pa and a second peak of 3 eV in the 0–20° range at 2 Pa, followed by a decrease to 500 eV at 10 Pa. The low kinetic group is described by a two-peak distribution throughout the plasma volume with a maximum of 80 eV at 10−2 Pa and a secondary peak at 190 eV at 2 Pa. The higher velocities derived in the N2 case are due to the plasma front acceleration of the plasma induced by the formation of a N− O+ charge separation. The ion density increases with the addition of N2, with two maxima of 1.7 × 1013 cm−3 at 2 Pa and 3.5 × 1013 cm−3 at 10 Pa. Noticeably, the angular split observed in the density distribution at 20° which starts at 10−2 Pa and remains a constant feature for all N2 pressures. When these results are combined with the XPS data, where no Mn–O–N bonds are visible, the N2 molecules are likely physically adsorbed on the surface of the films, hindering any subsequent oxidation of the films during deposition.
More information about the plasmas generated in the two regimes was obtained by implementing the technique from ref. 53 for the calculation of the electron temperature and plasma potential. As shown in Fig. S9 and S10, under low-O2 conditions, several Te maxima of 4.5 eV are observed at approximately 200 ns, 4.8 eV in the 2.5–3 μs range, and 4 eV in the 6 μs range. For higher pressures, only the contributions in the μs region are noticeable, with intense peaks at 2 and 6 eV being formed above 2 Pa in the <1 μs region. In the N2 case, a constant Te contribution ranging between 2.3 and 5.6 eV in the sub μs region is observed for all pressures, with a maximum in the 10−2–2 Pa region. A noticeable feature in the N2 case is a splitting of the maxima seen in the μs region below 10−2 Pa N2, followed by confinement of the structures at approximately 5 μs, which remains well defined even under high-pressure conditions. In both the N2 and O2 cases, a strong increase in the Vp value is observed at <500 ns: a maximum of 10 V is found for 10−2–10−1 Pa of N2 whereas a maximum of 14 eV is found in the 2–5 Pa O2 region. Similar to the temperature evolution in the 1–10 μs region, a secondary contribution is observed. In the N2 case, it ranges between 2.3 and 5 V, with the maximum shifting with increasing pressure from 10−4 to 2 Pa from 8 μs to 5 μs. In the case of oxygen in the same temporal region, a maximum of 5.3 eV is observed at 6 μs, which results in a shift toward longer evolution times above 2 Pa of O2 up to 20 μs. Importantly, the increase in both Vp and Te in the <500 ns range means that in front of the plasma, charges will have greater separation and thus accelerate along the expansion direction, whereas electrons will scatter due to collisions and thus increase the thermal energy of the plasma. The energetic balance shows that MnO molecular formation (386 kJ mol−1 formation enthalpy) in the gas phase can occur at low pressures (<10−3 Pa for N2 and <2 Pa for O2) in the 2–8 μs region but at high pressures in the <1 μs region. For low pressure, oxidation occurs in the core of the plasma, whereas with increasing O2 or N2 pressure, oxidation processes occur at the front of the plasma.
Supplementary information (SI) containing details on the structural and morphological properties of the thin films as well as extended plasma characterization. See DOI: https://doi.org/10.1039/d5tc03142g.
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